应用地球化学方法示踪地幔和地壳的形成过程和演化历史,探索固体地球的化学结构与层圈之间的相互作用,是化学地球动力学研究的前沿。
这些初步成果说明同位素填图与化学地球动力学在造山带研究中是具有重要前景的技术途径。
Theseachievements indicate that isotopic mapping and chemical geodynamics are significant and perspective approaches to researches on orogenic belts.
对流体-岩石相互作用过程中氧同位素变化的地球化学动力学进行了系统评述,其原理和模型也可扩展到对其他元素的研究。
This article reviews geochemical kinetics of oxygen isotope exchange during fluid rock interactions, whose principles and models can also be extended to studies on other elements.
本文通过岩溶特征分析和模拟试验研究,探索了岩溶形成演化环境及水文地球化学和水动力学蚀变模型。
Through the analysis of karst characters and study of simulated tests, the paper explores environment of formation and evolution of karst and hydrogeochemistry and hydrodynamic alteration model.
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